North Fork Blackwater River
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North Fork Blackwater River
The Blackwater River is a riverU.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed August 15, 2011 in the Allegheny Mountains of eastern West Virginia, USA. Via the Black Fork, it is a principal tributary of the Cheat River. Via the Cheat, the Monongahela and the Ohio rivers, it is part of the watershed of the Mississippi River and drains an area of . It is a true blackwater stream, owing to spruce and hemlock trees in its watershed, the tannins of which impart a tea or amber color to its water.Hissom, Patricia. 2006. "Blackwater River." ''The West Virginia Encyclopedia''. Ken Sullivan, editor. Charleston, WV: West Virginia Humanities Council. . Geography The entire course and drainage area of the Blackwater lie within Tucker County.DeLorme (1997). ''West Virginia Atlas & Gazetteer''. Yarmouth, Maine: DeLorme. . It rises on Canaan Mountain at an elevation of and initially meanders north-northeastwardly thr ...
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Blackwater Canyon
Blackwater Canyon is a rugged, heavily wooded, long gorge carved by the Blackwater River in the Allegheny Mountains of eastern West Virginia, USA. For many years, it has been the object of controversy as environmental activists have contended with industrial (power, timber, development) interests over its ultimate status. Description The canyon extends from the foot of Blackwater Falls near Davis to the confluence of the Blackwater River with Dry Fork (forming the Black Fork) near Hendricks, dropping about from to . It is a deep chasm separating Backbone Mountain (to the northwest) from Canaan Mountain (to the southeast). (This affords kayakers a whitewater river with Class IV-V+ pper Blackwaterand Class III-IV ower Blackwaterrapids). Tributary streamsnotably Pendleton Creek and Shay's Runhave formed hanging valleys high above the canyon floor. The land embracing the canyon consists of about of spruce, hemlock and pine upland, second-growth forest. Oak, maple, yello ...
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Eastern Hemlock
''Tsuga canadensis'', also known as eastern hemlock, eastern hemlock-spruce, or Canadian hemlock, and in the French-speaking regions of Canada as ''pruche du Canada'', is a coniferous tree native to eastern North America. It is the state tree of Pennsylvania. Eastern hemlocks are widespread throughout much of the Great Lakes region, the Appalachian Mountains, the Northeastern United States, and Maritime Canada. They have been introduced in the United Kingdom and mainland Europe, where they are used as ornamental trees. Eastern hemlock populations in North America are threatened in much of their range by the spread of the invasive Hemlock woolly adelgid, which infests and eventually kills trees. Declines in population from hemlock wooly adelgid infestation have led to ''Tsuga canadensis'' being listed as Near Threatened on the IUCN Red List. Eastern hemlocks are long lived trees, with many examples living for more than 500 years. They can grow to heights of more than , and are tol ...
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Blackwater River
A blackwater river is a type of river with a slow-moving channel flowing through forested swamps or wetlands. As vegetation decays, tannins leach into the water, making a transparent, acidic water that is darkly stained, resembling black tea. Most major blackwater rivers are in the Amazon Basin and the Southern United States. The term is used in fluvial studies, geology, geography, ecology, and biology. Not all dark rivers are blackwater in that technical sense. Some rivers in temperate regions, which drain or flow through areas of dark black loam, are simply black due to the color of the soil; these rivers are ''black mud rivers''. There are also black mud estuaries. Blackwater rivers are lower in nutrients than whitewater rivers and have ionic concentrations higher than rainwater. The unique conditions lead to flora and fauna that differ from both whitewater and clearwater rivers. The classification of Amazonian rivers into black, clear, and whitewater was fir ...
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Dry Fork (Cheat River)
The Dry Fork is a tributary of the Black Fork of the Cheat River in the Allegheny Mountains of eastern West Virginia, USA. Via the Black Fork, the Cheat, and the Monongahela and Ohio rivers, it is part of the watershed of the Mississippi River. The Dry Fork flows for much of its length in the Monongahela National Forest and drains mostly rural and forested areas.DeLorme (1997). ''West Virginia Atlas & Gazetteer''. Yarmouth, Maine: DeLorme. . It was traditionally considered one of the five Forks of Cheat. Name According to the Geographic Names Information System, Dry Fork has also been known historically as Dry Run. The stream's name derives from the occurrence of underground passages through which portions of the stream flow, leaving a dry streambed on the surface at times during the year. (See Sinks of Gandy) Geography Course The Dry Fork rises between Rich Mountain and Little Middle Mountain in eastern Randolph County and initially flows north-northeastwardly, past th ...
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Thomas, West Virginia
Thomas is a city and former coal town in Tucker County, West Virginia, United States. The population was 623 at the 2020 census. History Thomas was platted in 1884. Thomas was named for Thomas Beall Davis (1828-1911), brother of Senator Henry Gassaway Davis. The Davis brothers, in 1883, opened a mine near Thomas and had coal ready to ship when their railway arrived a year later. By 1892, Davis Coal and Coke was among the largest and best known coal companies in the world and employed 1,600 people. At the peak of its operations in 1915, there were nine producing mines within a mile of the company's office in Thomas. Immigrants flocked to the area as miners, railroad laborers, or merchants. The Company employed a man named Wladyslaw Dackiewicz as an interpreter. He could speak, read, and write eight languages and his services were much in demand with the influx of immigrants. In 1901, in less than two hours, nearly half of Thomas (83 buildings) was destroyed by a fire. The city w ...
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Whitewater
Whitewater forms in a rapid context, in particular, when a river's gradient changes enough to generate so much turbulence that air is trapped within the water. This forms an unstable current that froths, making the water appear opaque and white. The term "whitewater" also has a broader meaning, applying to any river or creek that has a significant number of rapids. The term is also used as an adjective describing boating on such rivers, such as whitewater canoeing or whitewater kayaking. Fast rivers Four factors, separately or in combination, can create rapids: gradient, constriction, obstruction, and flow rate. Gradient, constriction, and obstruction are streambed topography factors and are relatively consistent. Flow rate is dependent upon both seasonal variation in precipitation and snowmelt and upon release rates of upstream dams. Streambed topography Streambed topography is the primary factor in creating rapids, and is generally consistent over time. Increased f ...
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Blackwater Falls
Blackwater Falls State Park is located in the Allegheny Mountains of Tucker County, West Virginia, US. The centerpiece of the park is Blackwater Falls, a cascade where the Blackwater River leaves its leisurely course in Canaan Valley and enters rugged Blackwater Canyon. It is among the most photographed venues in the state and appears on calendars, stationery, and advertisements. The river is named for its tannin-darkened water. Geography Blackwater Falls State Park is located about two miles (3 km) southwest of Davis. It protects of red spruce and eastern hemlock upland forest. (Other important tree species in the park include yellow birch, American beech, red maple and black cherry.) The Falls The "Great Falls" of Blackwater River drop about at the head of Blackwater Canyon. The major ledge is composed of Connoquenessing sandstone of the Middle Pottsville Formation. The Falls are usually cited as the highest above-ground falls (there are higher cave falls) in the stat ...
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Waterfall
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which Erosion, erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is gen ...
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Canaan Valley National Wildlife Refuge
The Canaan Valley National Wildlife Refuge (CVNWR) in Tucker County, West Virginia, was the 500th National Wildlife Refuge (NWR) to be established in the United States. The refuge preserves a moist valley with unique wetlands and uplands at a relatively high elevation in the Allegheny Mountains. It is administered by the U.S. Fish and Wildlife Service (USFWS). History Advocacy for the establishment of a wildlife refuge in Canaan Valley began as early as 1961. In the 1970s, environmental and citizens' groups battled with Allegheny Power Systems (APS), which had owned more than of Canaan Valley since 1923, over construction of a long-anticipated hydroelectric facility that would have flooded about a quarter of the valley. In 1977, the Federal Power Commission issued a license to APS for construction of a pumped storage hydroelectric project, formally known as the Davis Power Project. However, the following year the Project was denied a Clean Water Act permit by the U.S. Army Co ...
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Canaan Valley Resort State Park
Canaan Valley Resort State Park is a state park in the eastern United States, within Canaan Valley in Tucker County, West Virginia. Located in the highest valley east of the Mississippi River, the park contains the second-largest inland wetland area in the United States. The valley featured the first commercial ski development in West Virginia. History In 1950 and 1951, members of the Washington Ski Club identified the Canaan Valley side of Cabin Mountain as an opportune place for ski development, based on pilots' reports. Because of its protection from the sun, snow on that side of the mountain often remains until April or later. The club began slope development in the early 1950s, signing a ten year operational lease with local landowners in 1954. Their slope, named Cabin Mountain Ski Area, featured two rope tows on of terrain stretching from route 32 to a height of . Runs extended down a slope with a vertical drop of . It was the first commercial ski establishm ...
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Canaan Valley
Canaan Valley () is a large bathtub-shaped upland valley in northeastern Tucker County, West Virginia, USA. Within it are extensive wetlands and the headwaters of the Blackwater River which spills out of the valley at Blackwater Falls. It is a well-known and partially undeveloped scenic attraction and tourist draw. Since 1994, almost 70% of the Valley has become the Canaan Valley National Wildlife Refuge, the nation's 500th National Wildlife Refuge, with Canaan Valley Resort State Park and Blackwater Falls State Park nearby. Canaan Valley was designated a National Natural Landmark in 1974. The National Park Service citation indicates that the Valley is "a splendid 'museum' of Pleistocene habitats ... contain ng... an aggregation of these habitats seldom found in the eastern United States. It is unique as a northern boreal relict community at this latitude by virtue of its size, elevation and diversity." The local pronunciation of "Canaan" is , rather than the conventional for ...
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